Predictive modelling of pH and dissolved metal concentrations and speciation following mixing of acid drainage with river water
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Discharge of acidic drainage from mining operations or acid sulphate soils can create severe environmental impacts if not managed appropriately. We tested different hydro-geochemical models to predict pH and dissolved Al, Fe and Mn concentrations and speciation following discharge and mixing of acid drainage into receiving waters; (1) an end member mixing approach using the geochemical model PHREEQC could accurately predict (r2>0.9) pH and dissolved metal concentrations at various dilutions over a pH range of 2-7, (2) dissolved inorganic and organic, and solid phase, Al and Fe speciation could be predicted using the geochemical model Visual MINTEQ (at 10% dilution), although poorer results were observed for Mn and drainage mixtures with lower metal concentrations, (3) PHREEQC gave similar results to a 3-D hydro-biogeochemical model (ELCOM-CAEDYM) when tested on a small-scale, and (4) ELCOM-CAEDYM successfully predicted dissolved metal concentrations (r2≥0.8), and to some extent pH (r2=0.2), over a 5month period in a 90km reach of the River Murray (South Australia) with over ten acid drainage discharges. The 3-D model was also used to assess river management scenarios and this highlighted a risk for dissolved Mn exceeding (aesthetic) drinking water guidelines in the river water at low flows. Limitations of the various models are discussed and we conclude that geochemical modelling is a useful tool to predict water quality impacts following discharge of acidic drainage to natural waters.
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Applied Geochemistry